Photographs by Jack Queen.
This season has not been kind to the ski resorts of Park City, Utah. Over block break, my friends and I encountered brown, bare mountains and dismally covered runs with tufts of grass peeking up between carved-out moguls. Base depth reports of 50 inches seem dubious at best given the snarls of rock plaguing many trails.
Unlike Colorado’s dry, slide-prone powder, Utah’s snow is generally much more stable, and steep couloirs in the Wasatch that would be unthinkable to ski in Colorado winter were good to go. The avalanche forecast was low for all aspects, save north facing slopes above treeline, and as we made our way up the canyon we giddily pointed out line after line descending from the jagged ridges.
No matter. A nice, steep line presented itself on the North aspect, so we ripped skins and dropped in. Here we encountered soft winter powder and linked together fluffy turns to the bottom of a small bowl, relishing the freedom such safe avalanche conditions provide.
Once the revelry was over, we shivered in the shade of the ridge. After hastily re-applying skins, we followed the track back to the ridge.
We then climbed to the high point of the ridge and decided we’d had enough skinning for one day. Picking our way down the other side of the ridge we found the entrance to Toledo Bowl and started our second and final run, a series of long, open pitches to the parking lot. The springtime snow on this aspect was a stark contrast to the power on the other side, and it felt as if we’d jumped forward in time to May.
At the parking lot we exchanged fist bumps, quads burning almost as much as our sun-cooked faces.
